母岩浆
The parental magma is basaltic magma, and its content of MgO is a little high, the content of MgO is 9.42%.
母岩浆为是MgO含量较高的玄武质岩浆,MgO含量为9.42%。
The pyroxenite xenoliths could be accumulates of the high-pressure fractional crystallization of the parental magma.
辉石岩类捕虏体是由该母岩浆高压分离结晶堆积的产物.
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